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自１９９２年４月１２日至１２月３０日对中山站以西内拉峡湾海冰和冰下水柱中藻类优势种组成和丰度进行了测定。４月份和１１月中旬至１２月中旬冰柱和水柱（０～５０ｍ）藻类丰度高达１０８～１０９ｃｅｌｓ／ｍ２。冰藻的普遍或季节性优势种主要包括Ａｍｐｈｉｐｒｏｒａｋｊｅｌｍａｎｉ、Ｂｅｒｋｅｌｅｙａｒｕｔｉｌａｎｓ、Ｎａｖｉｃｕｌａｇｌａｃｉｅｉ、Ｎｉｔｚｓｃｈｉａｂａｒｋｌｅｙｉ、Ｎ．ｃｙｌｉｎｄｒｕｓ、Ｎ．ｌｅｃｏｉｎｔｅｉ和Ｎｉｔｚｓｃｈｉａｓｐ．。由于藻类结合入冰后自身的演替，春－夏季海冰剖面中所记录的优势种组成并不能准确反映冰底优势种的季节演替过程。从冰底和水表藻种组成的对比表明，两者仅在春末冰底冰藻水华期间具有较强的相似性。秋、春季冰底冰藻水华的形成以现场生长为主，夏初冰藻释放入水后对冰下浮游植物的播种作用不明显。
From April 12 to December 30, 1992, the composition and abundance of dominant species of algae in sea ice and ice under water column in the west flank of the Zhongshan Station were measured. In April and mid-November to mid-December, the abundance of algae in icicles and water column (0-50 m) was as high as 108-109cels / m2. Common or seasonal dominant species of ice algae include Amphiprorakjelmani, Berkeleyarutilans, Naviculaglaciei, Nitzschiabarkleyi, N. cylindrus, N. lecointei and Nitzschiasp. . Due to the succession of algae after their incorporation into ice, the dominant species recorded in the spring-summer sea-ice profile can not accurately reflect the seasonal succession process of the dominant species in the ice. The comparison of the composition of algae species from the ice and water table shows that the two species have strong similarity only during the end of the spring ice cap algae blooms. The formation of glacial algae blooms in autumn and spring was dominated by on-site growth. The seeding effect of phytoplankton under ice was not obvious after the release of ice into the water in early summer.